erosion
A horn is typically the result of erosion where glaciers carve multiple slopes on a mountain peak, leaving a sharp, pyramid-like feature. The eroded cirque walls on all sides of the peak give it a distinctive shape.
A drumlin is a depositional landform, created by the deposition of glacial sediment underneath a moving glacier. It has a characteristic elongated shape with a steeper up-ice side and a gentler down-ice side.
High depositional environments include deltas, beaches, and river channels where sediments accumulate rapidly. In contrast, low depositional environments such as deep ocean basins, where sedimentation occurs slowly due to reduced sediment input and energy, leading to finer-grained deposits.
Depositional basins.
U-shaped valleys are a result of alpine glacial movement. Bedrock is scoured and plucked by continental glaciers. A number of depositional features are a result of the movement and depositing of rock, sand and dust associated with glaciers.
the erosion zone
Loess is primarily a depositional sediment, formed from fine particles of silt that are transported by wind and then deposited when the wind's velocity decreases. It typically accumulates in thick, blanket-like layers, often in areas lacking vegetation. While loess can be subject to erosion by wind and water, its formation process is fundamentally depositional.
The depositional features from the options provided are c) delta. A delta forms at the mouth of a river where sediment is deposited as the water slows down, creating landforms. A valley is a landform shaped by erosion and does not represent a depositional feature, while an aquifer is a geological formation that can hold water but is not a depositional feature. A river, on the other hand, is a flowing body of water and not a depositional feature itself.
No, a cliff is not a depositional feature; it is primarily an erosional feature. Cliffs are formed through the processes of erosion, where rock and soil are worn away by natural forces such as water, wind, or ice. This results in steep, vertical or near-vertical rock faces. Depositional features, on the other hand, are formed from the accumulation of sediment and materials, such as beaches and deltas.
Volcanoes are different from other mountains because they are built by deposits (magma), whereas other mountains are built by erosion. Volcanoes have lava, whereas other depositional mountains do not, even though they may have hot spots.
depositional
Deposition is when particals are dropped of and left. Erosion is where particales are carried away
Depletion of ozone causes UV to enter. They fall on ground and plants and kill them. Plants avoid erosion. Thus erosion is increasing because of it.
A depositional mountain is a landform created by the accumulation of sedimentary material, such as sand, gravel, or rock fragments. It forms when these materials are deposited over time, often by processes like erosion or the movement of glaciers, rivers, or wind. As the sediment builds up, it can eventually form a mountainous feature.
A horn is typically the result of erosion where glaciers carve multiple slopes on a mountain peak, leaving a sharp, pyramid-like feature. The eroded cirque walls on all sides of the peak give it a distinctive shape.
A drumlin is a depositional landform, created by the deposition of glacial sediment underneath a moving glacier. It has a characteristic elongated shape with a steeper up-ice side and a gentler down-ice side.
A deferred junction is typically associated with depositional landforms. It forms when sediment is deposited at the intersection of two rivers or streams, creating a more stable junction point.